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First Fossil Faorina (Echinoidea: Spatangoida) from the Bhuban Formation (Miocene), Northeastern India
Chia-Hsin Hsu, Lalramengi Fanai, Kongrailatpam Milankumar Sharma, Malsawmtluanga, J. Malsawma, Paul Lalnuntluanga, R. P. Tiwari, Rajeev Patnaik, Ammu Sankar Senan, Jih-Pai Lin*
Chia-Hsin Hsu
School of Ocean and Earth Science, University of Southampton, Southampton, SO14 3ZH, UK
chiahsinhsu01@gmail.com
Lalramengi Fanai
Department of Geology, Mizoram University, Mizoram, 796004, India
mami18fanai@gmail.com
Kongrailatpam Milankumar Sharma
Department of Geology, Central University of South Bihar, Gaya, 824236, India
milankumar.sharma@gmail.com
Malsawmtluanga
Lunglei Government College, Government of Mizoram, Mizoram, 796701, India
mstmzu.gps@gmail.com
J. Malsawma
Department of Geology, Mizoram University, Mizoram, 796004, India
jmvalpuia@gmail.com
Paul Lalnuntluanga
Department of Geology, Mizoram University, Mizoram, 796004, India
paultluanga@gmail.com
R. P. Tiwari
Department of Geology, Central University of Punjab, Bathinda, 151001, India
rptmzu@rediffmail.com
Rajeev Patnaik
Department of Geology, Panjab University, Chandigarh, 160014, India
rajeevpatnaik@gmail.com rajeevpatnaik@gmail.com
Ammu Sankar Senan
Department of Geosciences, National Taiwan University, Taipei, 106319, Taiwan
ammusankars93@gmail.com
Jih-Pai Lin
Department of Geosciences, National Taiwan University, Taipei, 106319, Taiwan
alexjplin@ntu.edu.tw
[We follow the code of the International Commission on Zoological Nomenclature, taxonomic papers with new species/genus descriptions will not have early view version.]
Communicated by Chien-Hsiang Lin

Heart urchins of the genus Faorina are now endemic to the Indo-West Pacific, but their fossils were previously known from the Miocene of Mediterranean, indicating a wider geographic distribution in the past. Here we describe Faorina mizoramensis sp. nov. from the Lower to Middle Miocene Bhuban Formation (Surma Group) in northeastern India, identified by their meridoplacous plating in interambulacrum 1 adorally. These fossils demonstrate that the distribution of Faorina had reached the eastern Indian Ocean (or Ceno-Tethys) by the Early to Middle Miocene. This study shows that Faorina likely expanded widely, extending into the Mediterranean during the Miocene. Following the closure of the Tethyan Seaway, they experienced local extinction. Today, they are restricted to Taiwan, southern China, Vietnam, Australia, Sulu Sea, Burma, and the Andaman Islands. We therefore hypothesize that Faorina may have originated in the Mediterranean, with the Indo-West Pacific later becoming a refugium for this genus and some of the tropical to subtropical Ceno-Tethyan echinoid faunas.  

Keywords

Biogeography, Systematics, Echinoidea, Irregularia, Spatangoids, Tethys  

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Citation:

Hsu CH, Fanai L, Sharma KM, Malsawmtluanga, Malsawma J, Lalnuntluanga P, Tiwari RP, Patnaik R, Senan AS, Jih-Pai Lin JP. 2026. First fossil Faorina (Echinoidea: Spatangoida) from the Bhuban Formation (Miocene), northeastern India. Zool Stud 65:21.

( Received 13 October 2025 / Accepted 07 March 2026 )